Isostatic Uplift

Isostatic Uplift is a geophysical process of crustal elevation resulting from the upward adjustment of the lithosphere in response to the removal of surface loads, such as ice or sediment, driven by gravitational equilibrium between the crust and the underlying mantle.

174

Publications

8.7K

Citations

458

Authors

225

Institutions

Publications per year

2017–2026

15

Authors

458

  1. NM
    Nils‐Axel Mörner

    Stockholm University, Sweden

    4 publications · 247 citations

    4

    h-index

  2. TP
    Tore Påsse

    Geological Survey of Sweden, Sweden

    4 publications · 201 citations

    4

    h-index

  3. MA
    Michel Allard

    Université Laval, Canada

    4 publications · 246 citations

    4

    h-index

  4. PS
    Per Sandgren

    Lund University, Sweden

    3 publications · 145 citations

    3

    h-index

  5. TO
    Tore O. Vorren

    UiT The Arctic University of Norway, Norway

    3 publications · 75 citations

    3

    h-index

1–5 of 458

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 12 publications · 758 citations

    12

    h-index

  2. Boreas

    10 publications · 481 citations

    10

    h-index

  3. Geological Society London Special Publications

    7 publications · 282 citations

    7

    h-index

  4. Tectonics

    7 publications · 451 citations

    7

    h-index

  5. Canadian Journal of Earth Sciences

    6 publications · 163 citations

    6

    h-index

1–5